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Bryophytes and their distribution in the Blue Mountains region of ...

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Cunn<strong>in</strong>ghamia 10(2): 2007 Down<strong>in</strong>g et al, <strong>Bryophytes</strong> <strong>in</strong> <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s 227<br />

Fig. 2. Section show<strong>in</strong>g geological strata <strong>and</strong> l<strong>and</strong>forms along (A) (B) (C) <strong>in</strong> Figure 1. (Modified from Geological Survey <strong>of</strong> New South<br />

Wales 1997)<br />

Climate<br />

Ra<strong>in</strong>fall is significantly higher <strong>in</strong> <strong>the</strong> upper mounta<strong>in</strong>s<br />

(1200–1400 mm p.a.) than <strong>in</strong> lower areas to <strong>the</strong> east <strong>and</strong> west<br />

(about 700–800 mm) (Table 1). The basalt peaks are high<br />

po<strong>in</strong>ts (above 1000 m a.s.l.) on <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s plateau,<br />

<strong>and</strong> correspond<strong>in</strong>gly <strong><strong>the</strong>ir</strong> ra<strong>in</strong>fall is higher than surround<strong>in</strong>g<br />

areas. Mount Tomah has an annual average ra<strong>in</strong>fall <strong>of</strong> 1541<br />

mm <strong>and</strong> probably similar ra<strong>in</strong>fall is experienced at <strong>the</strong><br />

o<strong>the</strong>r high peaks (Rodd 1987). Ra<strong>in</strong>fall is relatively evenly<br />

distributed throughout <strong>the</strong> year, but slightly lower <strong>in</strong> w<strong>in</strong>ter.<br />

Cloud, mist <strong>and</strong> fog are not uncommon <strong>and</strong> snow falls<br />

occasionally <strong>in</strong> w<strong>in</strong>ter on <strong>the</strong> higher parts above 1000 m.<br />

Temperatures <strong>in</strong> <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s are cooler both <strong>in</strong><br />

summer <strong>and</strong> <strong>in</strong> w<strong>in</strong>ter than those <strong>in</strong> Sydney (Table 1). In<br />

general, temperatures are higher <strong>in</strong> areas to <strong>the</strong> north-west<br />

<strong>of</strong> <strong>the</strong> area (eg Glen Davis) but ra<strong>in</strong>fall is much lower, about<br />

650 mm per annum. To <strong>the</strong> south, (Taralga) temperatures are<br />

close to those <strong>of</strong> <strong>the</strong> higher <strong>Blue</strong> Mounta<strong>in</strong>s, but ra<strong>in</strong>fall is<br />

lower, about 800–900 mm p.a. (Commonwealth Bureau <strong>of</strong><br />

Meteorology 2006).<br />

Table 1. Climatic Records for sites <strong>in</strong> <strong>and</strong> near <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s study area (Mount Tomah data from Rodd (1987), o<strong>the</strong>r sites<br />

from Commonwealth Bureau <strong>of</strong> Meteorology (2006)).<br />

Measurement Sydney Richmond Mt Tomah Katoomba Mt Victoria Lithgow Glen Davis Taralga<br />

Metres above sea level 39 19 1016 1030 1064 950 282 845<br />

Mean daily maximum<br />

temperature for<br />

January °C<br />

25.8 29.6 26.5 23.1 23.0 25.5 30.3 25.7<br />

Highest maximum<br />

temperature for<br />

January °C<br />

45.3 47.8 N/A 36.1 35.5 37.7 N/A 38.8<br />

Mean daily m<strong>in</strong>imum<br />

temperature for July °C<br />

8.0 3.6 3.6 2.5 1.7 0.7 2.0 0.6<br />

Lowest m<strong>in</strong>imum<br />

temperature for July °C<br />

2.2 -8.3 -5.0 -8.2 -6.3 -8.0 N/A -9.6<br />

Ra<strong>in</strong>fall mm per annum 1217 810 1541 1402 1061 863 634 804<br />

Cloudy days per annum 134 123 N/A 148 126 142 N/A 124

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